Gravity anomaly and fine crustal structure in the middle segment of the Tan-Lu fault zone, eastern Chinese mainland

Author:

Wang Xin,Jiang Wenliang,Zhang Jingfa,Shen Wenhao,Fu Zhihao

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference61 articles.

1. Crustal P-wave velocity structure in Lower Yangtze region: reinterpretation of Fuliji-Fengxian deep seismic sounding profile;Bai;Chin. Sci. Bull.,2006

2. Moho depth determinations based on spectral ratio analysis of NORSAR long period P-wave;Berteussen;Phys. Earth Planetary Interiors,1977

3. The N-W trending faults in middle part of Shandong province and their activities in the late Quaternary;Chao;J. Seismolog.,1992

4. Mode of motion the Holocene fault in Weifang-Jiashan segment of the Tanlu fault zone and earthquake-Generating model;Chao;J. Seismol. Res.,1997

5. A thinned lithospheric image of the Tanlu Fault Zone, eastern China: constructed from wave equation based receiver function migration;Chen;J. Geophys. Res. Solid Earth,2006

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